Method for compensating seismic detector signals for intersignal time variations



F. G. BLAKE ETAL July 1, 1958 2,841,777

METHOD FOR COMPENSATING SEISMIC DETECTOR SIGNALS FOR INTERSIGNAL TIME VARIATIONS Filed July 5, 1955 u Qmoumm INVENTORS FRANC/5 G. BLA/(E AUB/9A E.

LEY

ponents -retained. analysis, the original broadband record is analyzed'on the basis of a `variety of dilferent filter settings to deternited States Patent ce I2,841,777 Patented July 1, 1958 METHOD -FOR COMPENSATING SEISMIC DE- TECTOR SIGN ALS `FOR INTERSIGNAL TIME VARIATIONS Francis G. Blake and Auhra-E. Tilley, Fullerton, Calif., assignors Vto California Research' Corporation, San Francisco, Calif., acer-poration of Delaware Application July 5, 1955, Serial No. 519,876

4-Claims. (Cl. 340-15) 'be reproducibly recorded and subsequently `reproduced repeatedly and at will, usually in the laboratory, for further analysis. Reproducibly recording the `signals permits a number of different operations to be performed on thesignals to improve the signal-to-noise ratio or otherwiseincrease the information obtainable `from the signals.

One of `such operations utilized to aid in obtaining information from therecorded seismic data is the use of different lter settings on different playebacks of the records, the originalseismic detector signals having been recorded with ysubstantially vall of the original frequency com- Then, -in subsequent playback and mine 'the optimum filtering conditions.

yAnother operation sometimes utilized to `increase the signalto-noise ratio of 'the seismic detector signals is vmixing or combining different detector signals to produce a` composite signal in "which the reilectionsor other events of interest are more kprominent than in the unmixed signals. Inone suchmethod of mixing, signals produced by ldifferent seismic `detectors during a given seismic disturbance vare fmixed to vproduce a composite signal in which noise vpresent iin :each of the individual signals should, to some extent, vtend to randomize, with a consequent increase in the relative magnitude of the reections.

The mixing of more than one seismic record is often usefulinfbringing outldeep'reections which, in Va single record, are obscured by reverberation, by energyscattered from shallow inhomogeneities or `by high-frequency surface Waves, and a number of different types of interrecordmixing may be utilized to improve the information obtainable from vthe seismic prospecting. ln'one of lsuch methods, two separate seismic disturbances :are produced Vutilizing the same relative fpositions of shot point and detectors during both disturbances. Each ofthe resulting seismic detector signals from the first disturbance is then mixed or combined with the signal from the corresponding detector in the second disturbance to produce a group of composite signals.

In the above-described mixing operations, it is essential that time varlations between the arrivals of reflected energy from a given reflecting horizon at the different seismic detectors be compensated for prior Vto mixing so that corresponding reflections in the diiferent signals will be in the proper phase relationships to produce maximum reinforcement vof the reiiections in the composite signal. The intersignal or intertrace time variations in a seismic record may be divided into two categories-those which have a substantially constant value for the duration of a given seismic disturbance, and those whose'm'agnitude is variable throughout the duration of the v'seismic disturbance. Among the causes of the substantially constant time variations are differences in the thickness of -the weathered layer under the different detectors anddipping or tilting of a reliecting horizon. The most important cause of the variable time delays is the fact thatthe=diier ent detectors are spaced different distancesfrom theshot point or other source of seismic energy so that energy reilected from a given subsurface interface consequently arrives at the detector nearest the shot point before Kit arrives at detectors farther from the shot point. This latter time variation, commonly referred to as normal moveout time, has its maximum values for reilections from relatively shallow reflecting horizons, Asince the dilerences in the distances from the reecting `horizon to the different detectors are larger for these shallow reflections than for deeper reflections. Thus, the normal moveout time decreases in value during the seismic disturbance and becomes substantially zero when the diffe'rences in the distances from the reflecting horizon `to the diiferent detectors become negligible.

Broadly, the present invention contemplates `methods and apparatus for analyzing seismic detector signals in which a continuously Variable time correction is Aintroduced into each of the signals to compensate -for normal moveout time variations and a substantially xed correction is introduced into each of the signals vto compensate for fixed intersignal time variations. In lone embodiment, the seismic detector signals are recorded on va reproducible recording medium yand then yreproduced therefrom through reproducing heads which are movable Yrelative toeach other and to the recording medium. The

reproducing heads are driven from a normal moveout programming device which moves the different rreproducing heads during the reproduction operation in accordance with the normal moveout function obtaining in the surveyed area to remove the elfect ofnormal'rnoveout from the reproduced signals. Since the normal moveout correction varies nonlinearly during Vthe duration of the signals and also varies nonlinearl'y Vfrom `Signal to signal at any instant during the rst portion of the record, the normal moveout programming deviceproduce-s the non linear movement of the reproducing :heads required to introduce the desired correction. The reproduced signals, from which the'normal'moveout time variations have been removed, are then supplied to the movable recording heads of a second reproducible recording medium. The movable recording heads are shifted relative to each other along the Vtime axis of the recording medium by amounts corresponding to the amounts of `correction required to compensate for the substantially fixed time variations in the detector signals. The sig nals, as recorded on the second recording medium, will then have been corrected for both iixed and variable intersignal time variations, with the result that corresponding events or reflections in each of the signals will be substantially aligned in time, thus facilitating visual analysis of the signals and/or insuring that optimum reinforcement of corresponding reflections occurs when the signals `are mixed.

It is, therefore, an object of this invention to provide improved methods and apparatus for removing `time variations from a plurality of related seismic detector signals.

It is an additional object of the present invention to provide methods-and apparatus for accurately correcting a plurality of related seismic detector signals for variations in the time of occurrence of corresponding events in the signals by introducing into each of the signals a 3 time correction which has component of variable magnitude and a component of substatially fixed magnitude.

It is a further object of the present invention to provide methods and apparatus for accurately correcting a plurality of related seismic detector signals for variations in the times of occurrence of corresponding events in said signals by introducing into each of said signals a time correction which has a component of variable magnitude and a component of substantially fixed magnitude, the component of variable magnitude for a given signal varying nonlinearly during the duration of the signals.

It is a further object of the present invention to provide methods and apparatus for accurately correcting a plurality of related seismic detector signals for variations in the times of occurrence of corresponding events in said signals by introducing into each of said signals a time correction which has a component of variable magnitude and a component of substantially fixed magnitude, the component of variable magnitude for a given signal varying nonlinearly during the duration of the signals, and the component of variable magnitude varying nonlinearly from signal to signal at any instant during the rst portions of the signals.

Objects and advantages, other than those outlined above, will become apparent from the following detailed description taken in conjunction with the accompanying drawing, the single figure of which diagrammatically illustrates one embodiment of the present invention together with a cross-section of representative terrain to be surveyed.

The single figure illustrating the present invention shows av cross-section of representative terrain to be eX- plored by the method of this invention. A plurality of seismic detectors 11A, 11B, 11C, and 11D are shown at spaced-apart points on the surface of the earth for detecting seismic waves generated by a source of seismic energy generally designated 12. As is well known in the art source 12 may be an explosive material or an elevated weight which is dropped or any other suitable source of seismic energy. Source 12 produces waves which travel through the earth and are reflected from various subsurface interfaces back to the surface of the earth, where the earth movement is detected and converted into corresponding electrical signals by detectors 11A, 11B, 11C and 11D. Although, for simplicity, only four detectors are shown in the drawing, it will be understood by those skilled in the art that any suitable number of such detectors may be utilized and that the detectors may be arranged in any suitable known configuration.

The portion of the terrain shown in the figure is cornposed of a weathered layer 15, upon which the detectors are located, and subsequent strata 16, 17 and 18. Ideally, the energy radiated by source 12 and reflected by the interface between strata 16 `and 17 travels by paths P1, P2, P3 and P4, respectively, to the detectors 11A, 11B, 11C and 11D. Similarly, the energy reflected back to the detectors from the interface between strata 17 and 18 travels by paths P5, P6, P7, and P8 to the different detectors. It will be seen from the cross-sectional view of the terrain that the thickness of the weathered layer through which the different reflections travel is different for each of the detectors 11A, 11B, 11C and 11D. It is, therefore, necessary to correct for the effects of these different thicknesses of weathered layer on the travel times of the reflected energy to provide the proper phase relationships among the different signals for mixing. Substantially fixed time delays may also be caused by differences in the elevations of the different detectors or by dipping or tilted reflecting horizons, and these time delays, where present, will also require correction.

In making .the weathering corrections, it is possible to assume that they are the same for all directions of arrival of the waves, since the velocity of wave propagation through the weathered layer is very much lower than through the consolidated strata beneath it. As a result, the waves passing from the unuderlying stratum into the weathered layer are bent toward the vertical, and since the difference in velocity between the weathered layer and the underlying stratum is substantial, the error involved in assuming that the waves do travel vertically through the weathered layer is negligible. Therefore, the time delay component corresponding to the Weathering correction may be considered to be substantially constant for any given detector throughout the duration of the seismic disturbance.

An additional factor producing dillerences in the times of arrival of a given reflection at the different detectors is that the several detectors are different distances from the source 12. Thus, the reflection from the interface between strata 16 and 17, traveling path P1, will reach detector 11A before the energy reflected .from this same interface and traveling along path P2 arrives at detector 11B. The arrivals of the energy reflected from this interface will also be correspondingly delayed in arriving at detector 11C and at detector 11D. Similarly, the energy reflected from the interface between strata 17 and 18 will arrive at detector 11A before the energy reflected from this interface arrives at detector 11B, and will arrive at detectors 11C and 11D at correspondingly later times. However, the time delay or normal moveout time for the interface between strata 17 and 18 is not as large as the normal moveout time for the reflections Ifrom the interface between 16 and 17, since the differences in the distances traveled by the energy to the several detectors are smaller for reflections from the interface between strata 17 and 18 than for reilections from the interface between strata 16 and 17.

Thus, the normal moveout time is a function having its maximum value for reflections from shallow reilecting horizons and decreasing in value for subsequent reilections from deeper horizons, finally decreasing to substantially zero when the differences in the distances traveled by the different reflections from a given reflecting horizon to the several detectors are negligible. The exact shape of the moveout function as a function of the time after the initiation of the seismic disturbance will, of course, depend upon the particular velocity functions involved in the terrain being explored and the particular spacings of the detectors, but, in general, the moveout function appears to decrease somewhat exponentially as a function of the time elapsing after the shot.

From the above discussion, it will be apparent that the energy reaching the different detectors may be considered to have a time delay component which is substantially fixed throughout the duration of the seismic disturbance, and a time delay component which is variable in `magnitude throughout the duration of seismic disturbance. If the signals produced by detectors 11A, 11B, 11C and 11D are to be combined, it is essential that similar events or reflections in each of the different signals be in phase for such mixing in order to increase the magnitude of the reflection in the mixed signal relative to the surrounding noise. To accurately compensate for the different intertrace time variations, each of the signals should be varied in time relative to the others by an amount which has a substantially fixed component and a component which is variable during the duration of the signal.

To accomplish this, the different output signals from the detectors lare supplied through an amplifying network 21 to a suitable reproducible recording device generally designated as 22. Recording device 22 may be of any suitable known type, but, preferably, it is a magnetic recording device having a layer of magnetizable material 24 mounted on a rotor driven by a motor 25. Recorder 22 is also provided with a plurality of recording heads 22A, 22B, 22C and 22D connected, respectively, to the several detectors 11B, 11C and 11D 'the recorded signals.

5 through'amplifer '21. Device :22 may be also rprovided with 'a plurality of reproducing or playback heads 23A, 23B, 23C and 23D, corresponding, respectively, to 'recording heads 22A, 22B, 22C and l22D, for reproducing the information recorded on the diEerent channels of magnetizable layer 24. Although separate recording heads and reproducing heads for each channel have been `shown in the drawing, Ait will Vbeobvious to ythose skilled in 'the art that these ztwo functions may -be `combined in a single head for each channel, and such variation is contemplated Vas being within the scope of this invention.

Each of heads 23A, 23B, 23C and 23D is movable about the periphery of layer 24 so as to vary the krelative positions of each :of 'these heads along the time axis of The reproducing heads are rnechanically connected, asshown by the dotted lines, to a device 36 for moving the reproducing heads according to a predetermined pattern or program during the reproducing 'operatio'tn as will be discussed more in detail below. The signals from the reproducing heads are supplied through an amplifying network 32, which may also contain a stage or stages of filtering, to a device 33 for transferring the reproducedrsignals to an intermediate storage device ygenerally designated 36.

Device 36 is preferably provided with a magnetic recording medium, such as a magnetizable layer 37 upon which aplurality of recording heads 36A, 36B, 36C and 36D records signals supplied thereto. 'The storge capacity of intermediate storage device 36 is preferably considerabl-y in excess of the storage capacity of recorder 22 so that several groups `of signals loriginally recorded on device 22 may be simultaneously stored on intermediate storage device 36. Intermediate storage device 36 is alsoprovided withreproducingheads 38A, 38B, 38C and 38D for reproducing the associated signals recorded by the recording heads. The reproducing heads of device 36 are movable about the periphery `of layer 37 so as to enable the positions of the reproducing heads to be varied along the time axis ofthe signals recorded on the different channels. As in the case of recording device 22, although separate recording heads and reproducing 4heads are Shown for each channel of device 36, it will be understood that the double function may be combined into a single head for each channel, as is well known in the art. The signals from reproducing heads 38A, 38B, 38C and 38D are connected to a signal processing network 41 in which additional operations, such as mixing, signal level adjustment, and filtering, may be performed on the reproduced signals. The output'from signal processing means 41 is supplied to a recording device 42 and/or a display device 43 for pro- -ducing a permanent record and/or an oscilloscopio display of the resultant composite signal or signals.

Device 36 is provided with means 4for accurately determining the speed `and position of the information recorded on the magnetizable layer 37. Such means may be in the form of a timing trace consisting of a series of notches Yor grooves 46 on one channel of device 36. Timing grooves -46 pass under a reproducing head 46A to supply a series of timing pulses yto a network shown schematically at 47 for controlling the relative speeds of rotation of devices 22 and 36 and for controlling the transfer of groups of seismic detector signals from device 22 to intermediate storage device 36. One or more of notches-46 maybe given a distinctive characteristic to provide an indication of the rotative position of recording medium 37. For example, the characteristic notch may be placed on medium 37 coincident with the beginning or Zero point in the time axis of medium 37, so that an indication is .provided when this point passes under head 46A. A device 48 driven in common with recording medium 24 by motor 25 is provided to produce a signal responsive to the speed and position of recording -medium a24. This signal is supplied to network 47 `Where itis compared withthesignal :from head 46A to provide the two recording media.

The signal vfrom network -47 is supplied to drive-motor 25 for correcting the speed and phase of 'recording medium 24 to the desired value. When the two recording media have the desired relative speedand phase relationships, network 47 supplies an kimpulse to actuate Vsignal transfer means 33 to transfer the group -of seismic detector signals from recording medium 24 to intermediate storage device 36.

The operation of ythe embodiment Yillustrated in the figure is as follows. yUpon actuation of source 12, energy is transmitted through the earth and reflected from the various reflecting'horizons back to detectors 11A, 11B, 11C and l11D to produce a plurality of VVelectrical signals varying in sympathy with the earth movement. As discussed above, reflections arriving at the 'different detectors from the different reflecting interfaces are subject to relative time delays, each of which may be considered to have a component which is of substantially constant magnitude throughout the duration of the seismic disturbance and a component having a magnitude variable during the duration of the seismic disturbances. The signals from the several detectors are amplified in amplifying network 21 and supplied to recording heads 22A, 22B, 22C, and 22D for recording on `the various channels of recording medium 24. The signals are preferably recorded with little or no filtering so that the original broad-band signals are available on recording medium 24 for subsequent analysis.

In the embodiment illustrated in the drawing, it has been assumed that the normal moveout is to be removed from the seismic signals during their reproduction from recorder 22 through reproducing heads 23, but it Will be obvious to those skilled in the art that the normal moveout may also be removed atany one of a number of other stages during the `processing operation. For example, the normal moveout could be removed during the initial recording stage by connecting normal moveout programmer 31 to recording heads 22A, 22B, 22C, and 22D and driving these recording heads from the programmer during the initial recording operation. However, this method would have the disadvantage that the original seismic signals would not be available for inspection or examination since the normal moveout would be removed prior 'to vthe original recording. Alternatively, the normal moveout removal could be performed when the seismic signals are recorded on recorder 36. In such 'a case, normal moveout programmer 31 would be connected to recording heads 36A through 36H to drive these heads in accordance with the normal moveout function during the reproduction of the original traces from recorder 22. As van additional alternate, the normal moveout removal operation could be performed when the signals are being reproduced frorn recorder 36 through reproducing heads 38A through 38H by connecting normal moveout programmer 31 to these reproducing lheads and reproducing the signals therethrough. In a similar manner, the fixed time compensations for the signals may be introduced at any desirable stage in the signal processing operation to compensate for weathering and elevation differences, step-out and other fixed time corrections.

lf intermediate storage device is adjacent recorder 22, the signals recorded on medium l24 may then Abe reproduced through heads 23A, 23B, 23C, and 23D. Usually, however, the field recorder is remote from the intermediate storage device, and in such cases, recording medium 24 is removed from the recorder and placed on a similar device located adjacent the intermediate storage device for reproduction of the signals. ln a representative operation, a plurality of tapes are recorded in the field and then Vtaken into the laboratory or field ofiice for analysis. ln such a case, a device substantially identical to recorder 22 and having reproducing heads 23A, 23B, 23C, and 23D is provided on ywhich the tapes may be placed for reproduction of the signals recorded thereon and transfer to intermediate storage device 36. During such reproduction, the reproducing heads are driven from. normal moveout programmer 31 in a predetermined fashion to compensate each of the different signals for the variable time delay component caused by normal moveout. As stated above, the normal moveout correction time, as a function of the time after initiation of the explosion, varies nonlinearly along each signal from a'maximum value to substantially zero for values of time corresponding to the times of arrival of deep reections, the exact configuration of this function depending upon the detector spacings and the particular velocity function obtaining in the area under study. The normal moveout correction also varies nonliuearly from signal to signal during the first portion of the seismic reco-rd, so that it is desirable that normal moveout programmer 31 provides both the nonlinear correction along each signal and the nonlinear corrections required from signal to signal during the early portion of the record.

Programmer 31 may be of any suitable type capable of providing required nonlinear drive for the reproducing heads in accordance with the desired normal moveout function. For example, reproducing heads may be individually driven by elements of programmer 31 or may be driven from a master output shaft whose movement is modified by appropriate cams for each of the different heads. Alternatively, programmer 31 may be a closed-loop-type servo network in whichl a quantity representing the actual position of the reproducing heads is compared with a quantity corresponding to the desired position of the reproducing head, and the difference between the two compared quantities is utilized to drive the reproducing heads to the desired position.

The diterent signals are thus reproduced through the reproducing heads with normal moveout removed. During the reproduction of the traces from recorder 22, recorder 22 is synchronized with the fixed timing marks 46 on recorder 36 to insure recording the signals on recorder 36 in the proper positions relative to the xed timing marks 46. These signals are then supplied through amplifying and/ or filtering network 32 and signal-transfer network 33 to recording heads 36A, 36B, 36C, and 36D to record the normal moveout-corrected signals on four of the channels of intermediate storage device 36. If only these four signals are to be mixed, they may be then reproduced through reproducing heads 38A, 38B, 38C, 38D. As stated above, the reproducing heads of device 36 are shiftable along the time axis of the recorded signals to compensate for the substantially constant time delays among the different signals. With the effects of normal moveout removed, and compensation made for the substantially fixed intertract time variations such as weathering and elevation differences, the arrivals of energy reflected from a given reflecting horizon should be coincident in time in all of the reproduced signals` These reproduced signals may then be mixed in signal processing network 41 in a manner which produces maximum reinforcement of each of the reflections present, with a consequent increase in signal level relative to noise level. The output from signal processing network 41 is supplied to recorder 42 to produce a permanent record of the composite signal produced by the mixing, and this output may also be supplied to display device 43 for producing a visual display for a rapid evalution of the effects of the mixing.

Assuming that it is desired to utilize the apparatus shown in the ligure in connection with the mixing of groups of seismic detector signals produced by more than one seismic disturbance, the operation would be as follows. For example, assume that after recording the group of seismic detector signals produced by detectors 11A, 11B, 11C and 11D in response to energy produced by source 12, as described above, the shot point and detectors are moved to the locations designated in Fig. 1

by reference characters 12', 11A', 11B', 11C' and 11D', respectively. It will be seen from the figure that the energy paths from source 12' to detectors 11A', 11B', 11C' and 11D will be of substantially the same lengths as the respective paths from source 12 to `detectors 11A, 11B, 11C and 11D except for the varying thickness of weathered layer 15. Thus, the signal produced by detector 11A should correspond fairly closely with the signal produced by detector 11A', and this correspondence should similarly obtain for signals from detectors 11B and 11B', detectors 11C and 11C', and detectors 11D and 11D.

However, the noise present in corresponding signals produced by the two spreads, particularly that noise which is spatial in character, such as that produced by reflections from near-surface boulders or caverns, would not tend to correspond between the two signals, so that mixing of the corresponding signals should randomize the noise to some extent and consequently reinforce the reflections. As will be well understood, this procedure is but one of the many types of inter-record mixing which may be utilized in an attempt to randomize noise or otherwise increase the signal-to-noise ratio of the detector signals.

Assuming that the group of signals produced by detectors 11A, 11B, 11C and 11D has been recorded on recording medium 24 and transferred into intermediate storage device 36, recording medium 24 is again available for recording. In this connection, it will be noted that, for the specific embodiment shown in the figure, no moveout correction is required in mixing corresponding signals from the two groups of signals, assuming that the detectors are equally spaced from each other and from the shot point in both spreads, since the arrival times at corresponding detectors in the two spreads for a reflection from any given interface should be the same for both spreads except for the effects of differences in weathered layer thickness or elevation of the detectors. Thus, the group of signals produced by detectors 11A, 11B, 11C and 11D could be recorded on recorder 22, reproduced therefrom and transferred through network 33 to intermediate storage device 36. However, if the dierent geophone spreads are not symmetrical, corrections for normal moveout would be required.

Source 12 may then be activated to produce seismic energy which is converted by detectors 11A', 11B', 11C and 11D' into electrical signals supplied through amplifier 21 to recorder 22. As stated above, it is necessary that the second group of detector signals recorded on intermediate storage device 36 be accurately positioned relative to the first group of signals stored thereon so that all of the signals are precisely aligned in time for mixing. To control the transfer of this second group of signals from recorder 22 to device 36, the signal produced by timing grooves 46 on storage device 36 is compared in network 47 with the signal produced by device 48 in response to the speed and position of recording medium 24. Network 47 compares these two values and supplies an error or correcting signal to motor 25 to bring the speed of this motor to the desired value.

When the two recording media have the desired speed and phase relationships, network 47 supplies a pulse to signal-transfer network 33 which gates the group of signals from recorder 22 into the storage bank of intermediate storage device 36 represented by recording heads 36E, 36F, 36G and 36H. Both groups of seismic detector signals are thus accurately positioned relative to each other on the storage surface of intermediate storage device 36, .and all of the signals may be reproduced by reproducing heads 38A through 38H with accurate time alignment therebetween. The different reproducing heads of device 36 may be shifted different amounts to compensate for intertrace time variations caused by differences in the thickness of the Weathered layer under the dif- 9 ferent detectors, dipping reecting beds, and/or differences in the elevations of the detectors.

The reproduced signals are supplied to signal processing network 41 where, for the particular type of inter-record mixing discussed above, the outputs from reproducing heads 38A and 38E, corresponding to the signals from detectors 11A and 11A', are connected together; reproducing heads 38B and 38F, corresponding to the signals from detectors 11B and 11B', are connected together; reproducing heads 38C and 3BG, corresponding to the signals from detectors 11C and 11C', are connected together; and reproducing heads 38D and 38H, corresponding to the signals from detectors 11D and 11D', are connected together. The signals are thus mixed to produce a composite record of four traces or signals, and these composite signals are applied to recorder 42 and/or display device 43.

Although but a few embodiments of the present invention have been illustrated and described, it will be obvious to those skilled in the art that various changes and modifications may be made therein without departing from the spirit of the invention or the scope of the appended claims.

We claim:

1. Apparatus for analyzing seismic data in the form of a plurality of groups of electrical signals, each of said groups being produced by a plurality of seismic detectors actuated by movement of the earth in response to a seismic disturbance, comprising a first rotatable, reproducible recording medium for sequentially recording each of said groups of signals, a second rotatable, reproducible recording medium having a recording capacity suicient to simultaneously record all of said groups of signals, transfer means connected between said first and said second media for transferring each of said groups of signals from said first medium to said second medium, normal moveout removing means connected to said first medium for introducing into the signals reproduced from said first medium time corrections correspond ing to the normal moveout corrections for said signals, means responsive to the speeds of rotation of said rst and said second recording media for actuating said transfer means upon synchronization of the speeds of said media to transfer said normal-moveout corrected signals to said second medium, means for reproducing said signals from said second recording medium with different time delays therebetween corresponding to the fixed time corrections for said signals, and means for selectively combining said signals reproduced from said second medium to produce a plurality of composite signals.

2. Apparatus for analyzing seismic data in the form of a plurality of groups of electrical signals, each of said groups being produced by a plurality of seismic detectors actuated by movement of the earth in response to a seismic disturbance, comprising a rst rotatable, reproducible recording medium for sequentially recording each of said groups of signals, a second rotatable, reproducible recording medium having a recording capacity sufiicient to simultaneously record all of said groups of signals, transfer means connected between said rst and said second media for transferring each of said groups of signals from said first medium to said second medium, normal moveout removing means connected to said first medium for introducing into the signals reproduced from said rst medium continuously varying time corrections corresponding to the normal moveout correction for said signals, means responsive to the speeds of rotation of said rst and said second recording media for actuating said transfer means upon synchronization of the speeds of said media to transfer said normal-moveout corrected signals to said second medium, means for reproducing said signals from said second recording medium with different time delays therebetween corresponding to the fixed time corrections for said signals, and means for selectively combining said signals reproduced from said second medium to produce a plurality of composite signals.

3. Apparatus for analyzing seismic data in the form of a plurality of groups of electrical signals, each of said groups being produced by a plurality of seismic detectors actuated by movement of the earth in response to a seismic disturbance, comprising a first rotatable, reproducible recording medium form sequentially recording each of said groups of signals, normal moveout removing means connected to said first medium for introducing into the signals recorded on said first medium time corrections corresponding to the normal moveout correction for said signals, a second rotatable, reproducible recording medium having a recording capacity suicient to simultaneously record all of said groups of signals, transfer means connected between said rst and said second media for transferring each of said groups of signals fromsaid first medium to said second medium, means responsive to the speeds of rotation of said first and said second recording media for actuatingvsaid transfer means upon synchronization of the speeds of said media to transfer said normal-moveout corrected signals to said second medium, means for reproducing said signals from said second recording medium with different time delays therebetween corresponding to the fixed time corrections for said signals, and means for selectively combining said signals reproduced from said second medium to produce a plurality of composite signals.

4. Apparatus for analyzing seismic data in the form of a plurality of groupsof electrical signals, each of said groups being produced by a plurality of seismic detectors actuated by movement of the earth in response to a seismic disturbance, comprising a rst rotatable, reproducible recording medium for sequentially recording each of said groups of signals, normal moveout removing means connected to said first medium for introducing into the signals recorded on said first medium time corrections corresponding to the normal moveout correction for said signals, a second rotatable, reproducible recording medium having a recording capacity suflicient to simultaneously record all of said groups of signals, transfer means connected between said first and said second media for transferring each of said groups of signals from said rst medium to said second medium, means responsive to the speeds of rotation of said rst and said second recording media for actuating said -transfer means upon synchronization of the speeds of said media to transfer said normal-moveout corrected signals to said second medium, means for introducing into said signals recorded on said second recording medium different time delays corresponding to the iixed time corrections for said signals, means for reproducing said signals from said second medium, and means for selectively combining said signals reproduced from said second medium to produce a plurality of composite signals.

References Cited in the le of this patent UNITED STATES PATENTS 2,243,730 Ellis May 27, 1941 2,638,402 Lee May 12, 1943 2,440,971 Palmer May 4, 1948 2,732,025 Lee Jan. 24, 1956 

